GIG OpenIR  > 同位素地球化学国家重点实验室
Xiong, Fahui1; Yang, Jingsui1; Robinson, Paul T.1; Xu, Xiangzhen1; Liu, Zhao2; Zhou, Wenda3; Feng, Guangying1; Xu, Jifeng4; Li, Jie4; Niu, Xiaolu1
High-Al and high-Cr podiform chromitites from the western Yarlung-Zangbo suture zone, Tibet: Implications from mineralogy and geochemistry of chromian spinel, and platinum-group elements
Source PublicationORE GEOLOGY REVIEWS
ISSN0169-1368
2017
Volume80Pages:1020-1041
DOI10.1016/j.oregeorev.2016.09.009
Language英语
WOS Research AreaGeology ; Mineralogy ; Mining & Mineral Processing
WOS IDWOS:000387625800056
Citation statistics
Cited Times:23[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/34986
Collection同位素地球化学国家重点实验室
Corresponding AuthorXiong, Fahui
Affiliation1.Chinese Acad Geol Sci, Inst Geol, Ctr Continental Dynam, CARMA, Beijing, Peoples R China
2.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China
3.China Univ Geosci, Fac Earth Sci, Wuhan 430074, Peoples R China
4.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochem, Guangzhou 510640, Guangdong, Peoples R China
Recommended Citation
GB/T 7714
Xiong, Fahui,Yang, Jingsui,Robinson, Paul T.,et al. High-Al and high-Cr podiform chromitites from the western Yarlung-Zangbo suture zone, Tibet: Implications from mineralogy and geochemistry of chromian spinel, and platinum-group elements[J]. ORE GEOLOGY REVIEWS,2017,80:1020-1041.
APA Xiong, Fahui.,Yang, Jingsui.,Robinson, Paul T..,Xu, Xiangzhen.,Liu, Zhao.,...&Niu, Xiaolu.(2017).High-Al and high-Cr podiform chromitites from the western Yarlung-Zangbo suture zone, Tibet: Implications from mineralogy and geochemistry of chromian spinel, and platinum-group elements.ORE GEOLOGY REVIEWS,80,1020-1041.
MLA Xiong, Fahui,et al."High-Al and high-Cr podiform chromitites from the western Yarlung-Zangbo suture zone, Tibet: Implications from mineralogy and geochemistry of chromian spinel, and platinum-group elements".ORE GEOLOGY REVIEWS 80(2017):1020-1041.
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